Also facing elimination are the Orbiting Carbon Observatory 3, which would observe carbon dioxide flows; a mission to the space station that would have supported tests of a spectrometer intended to measure solar reflection; and Plankton, Aerosol, Cloud, ocean Ecosystem, a satellite that would measure the colors of the ocean to gauge the global flow of algae and the influence of ocean
aerosols on cloud formation.
Joe Ceonnia: ``... it seems to me as if this program is all over the globe» Joe, by observing the astoundingly unnatural patterns of atmospheric
aerosols on cloud formations around the planet — via NASA Worldview (online)-- one can visibly observe the effects of geoengineering around the world.
Not exact matches
The
aerosols catalyze the
formation of ice in the
clouds, which could increase precipitation, although more research needs to be done
on that linkage, Creamean said.
Despite its smaller ash
cloud, El Chichn emitted more than 40 times the volume of sulfur - rich gases produced by Mt. St. Helens, which revealed that the
formation of atmospheric sulfur
aerosols has a more substantial effect
on global temperatures than simply the volume of ash produced during an eruption.
At least over the oceans, the pre-industrial
cloud conditions would have been considerably different from those of today; this implies that the
aerosols we have been adding to the atmosphere may have had a significant effect
on global patterns of
cloud formation and rain.
«Huge amounts of
aerosols from Asia go as high as six miles up in the atmosphere and these have an unmistakable impact
on cloud formations and weather.»
They found that galactic cosmic rays exert only a small influence
on the
formation of sulphuric acid — dimethylamine clusters (the embryonic stage before
aerosols may act as
cloud condensation nuclei).
However, I am not optimistic — the specifics of the small scale physics (
aerosol indirect effects
on clouds, sea ice
formation, soil hydrology etc.) are so heterogeneous that I don't see how you can do without calculating the details.
Perhaps the thresholds for a CRF -
cloud correlation was higher then than it has been for the past 40 years (one might imagine that in periods where the air is rather clear of man made
aerosols, the threshold for CRF effects
on cloud formation become higher... and so
on).
This paper re-states the grand Svensmark theory and attempts to address the work that has shown cosmic rays can not be a significant influence
on climate because most
aerosols run out of stuff to become big enough for
cloud formation.
In summary the findings to date indicate that the effect of cosmic rays
on cloud formation is small compared to the large variations in natural biogenic
aerosol emissions.
Romakkaniemi, S., Maalick, Z., Hellsten, A., Ruuskanen, A., Väisänen, O., Ahmad, I., Tonttila, J., Mikkonen, S., Komppula, M., and Kühn, T.:
Aerosol — landscape —
cloud interaction: signatures of topography effect
on cloud droplet
formation, Atmos.
If a
cloud doesn't form then because of lack of
aerosols to start
formation, chill that sucker down some more to form ice crystals and it should make its
on substrate to form.
The 2014 Biogenic
Aerosols — Effects
on Clouds and Climate (BAECC) field campaign in Finland has provided rich data
on processes related to
aerosol,
cloud, and snow
formation.
With
cloud tops warmer than -38 degrees Celsius, ice
formation depends
on aerosols that preferentially freeze at warm temperatures, referred to as ice nuclei.
The Indirect and Semi-Direct
Aerosol Campaign (ISDAC) field campaign, deployed from Barrow, Alaska,
on a Canadian National Research Council Convair - 580 jet in April 2008, provided improved observations of two new cases of single - layer, mixed - phase, stratiform
clouds that are well - suited to test our understanding of ice
formation.
These
clouds then glaciate in higher levels, which could result in either more or less vigorous precipitation
formation depending
on the background
aerosol levels and atmospheric stability (Khain et al., 2004).
On the other hand, if some of the anthropogenic
aerosols act as ice nuclei, supercooled
clouds could be converted into ice
clouds by the glaciation indirect effect (Lohmann, 2002), resulting in more efficient precipitation
formation.
It has been hypothesized that galactic cosmic rays (GCR) create atmospheric ions which facilitates
aerosol nucleation and new particle
formation with a further impact
on the
cloud formation (Kazil et al., 2012; Pierce and Adams, 2009).
In the article «Global atmospheric particle
formation from CERN
CLOUD measurements,» sciencemag.org, 49 authors concluded «Atmospheric
aerosol nucleation has been studied for over 20 years, but the difficulty of performing laboratory nucleation - rate measurements close to atmospheric conditions means that global model simulations have not been directly based
on experimental data.....
Under strict temperature and humidity conditions, investigations in this laboratory provide new information
on the particular
aerosol particles that can lead to the
formation of these
clouds.
Chamber research is focused
on understanding the lifecycle of organic
aerosols, including their
formation, growth, aging (oxidation), re-volatilization, and effect
on cloud formation.
BAECC was designed to obtain important details
on processes related to
aerosol,
cloud, and snow
formation that are not currently well understood or well represented in earth system models.
Topics that I work
on or plan to work in the future include studies of: + missing
aerosol species and sources, such as the primary oceanic
aerosols and their importance
on the remote marine atmosphere, the in -
cloud and
aerosol water aqueous
formation of organic
aerosols that can lead to brown carbon
formation, the primary terrestrial biological particles, and the organic nitrogen + missing
aerosol parameterizations, such as the effect of
aerosol mixing
on cloud condensation nuclei and
aerosol absorption, the semi-volatility of primary organic
aerosols, the importance of in - canopy processes
on natural terrestrial
aerosol and
aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of
aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance
on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect
on key gas - phase species like ozone + the physical and optical properties of
aerosols, which affect
aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing
aerosols +
aerosol -
cloud interactions, which include
cloud activation, the
aerosol indirect effect and the impact of
clouds on aerosol removal + changes
on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the
aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic
aerosol changes in the atmosphere
on the terrestrial biosphere, the ocean and climate.